Variation of carbon-14 isotope effect with substituent and the

Variation of carbon-14 isotope effect with substituent and the mechanism of the m-chloroperbenzoic acid ... Billy W. Palmer, and Arthur Fry ... Robert...
0 downloads 0 Views 280KB Size
2580

The photochemical rearrangements of 1 are subject to at least three interpretations: (i) initial formation of an excited diradical(4), which then serves as a common intermediate forming 3 by further bond cleavage and 2 by the appropriate radical recombination; (ii) formation of 2 via 4 as described above, accompanied by

Table I. Rates and Carbon-14 Kinetic Isotope Effects for the Oxidation of para-Substituted A~etophenones-l-l~C with m-Chloroperbenzoic Acid in Chloroform a t 32' para substituent

k X IO3,= 1. mol-' sec-1

k 2/k esterb

k12/k" ketone*

CHaO CH3

40.3 19.1 4.53 3.39 0.50

0.998 1.032 1.048 1.049 1.084

0.998 1.033 1.048 1.052 1.085

H c1 4

CN

5

+

an independent process involving a retro (2 2) T reaction giving cis,trans,cis,trans-cyclooctatetraene13 (S), which is converted to all-cis-cyclooctatetraene under the reaction conditions (even at - 60", attempts t o detect the intermediate formation of 5 were unrewarded, although experiments at much lower temperatures might yield different results)) (iii) formation of 2 from 1 via a concerted suprafacial [ 1,3] sigmatropic shift, and formation of 3 by one of the above-described paths. In any event, since the thermal rearrangement of 1 to 2 (unaccompanied by 3) seems to proceed via the corresponding diradical intermediate, the photochemical production of 3 from 1 must involve either a different state of this diradical or else some alternative mechanism. (13) Known compounds similar to 5 include trans,rrans-1,5-cyclooctadiene" and a trans,cis,cis,cis-cyclooctatetraenederivative. 16 (14) G. M. Whitesides, G. L. Goe, and A. C. Cope, J . Amer. Chem. Soc., 91, 2608 (1969). (15) E. H. White, E. W. Friend, Jr., R. L. Stern, and H. Maskill, ibid., 91,523 (1969).

Jerrold Meinwald, Haruki Tsuruta Department of Chemistry, Cornell Unifiersity Ithaca, New York 14850 Receioed February 16, 1970

Variation of Carbon-14 Isotope Effect with Substituent and the Mechanism of the rn-Chloroperbenzoic Acid Oxidation of Labeled para-Substituted Acetophenones' Sir: Small variations in heavy atom (nonhydrogen) isotope effects with ring substituents have been reported2 in the past, but in no case has changing ring substitution resulted in an isotope effect change from near the lower detectable limit to near the maximum expected. Except for the recent work of Yukawa, et u I . , ~ which was interpreted in terms of a changing mechanism with changing substituent, all previous studies of substituent effects on isotope effects have been carried out in systems in which the isotopic fractionation was taking place at an atom external to the ring bearing the substituent. We wish to present here the results (see Table I) of a series of kinetic and isotope effect measurements on the m-chloroperbenzoic acid oxidation of para-substituted acetophenones-1 - 14C (1) to pura-substituted (1) Supported by U. S. Atomic Energy Commission Contract ATfrom the Ph.D. Dissertation of B. W. P., University of

(40-1)-3234;

Arkansas, Fayetteville, Ark., 1970. (2) J. W. Hill and A. Fry, J . Amer. Chem. Soc., 84, 2763 (1962); J. Bron and J. B. Stothers, Can. J . Chem., 46, 1435 (1968); 47, 2506 (1969); A. N. Bourns and P. J. Smith, Proc. Chem. SOC.London, 366 (1964); G. A. Ropp and V. F. Raaen, J . Chem. Phys., 20, 1823 (1952); 22, 1223 (1954); C. G. Mitton and R. L. Schowen, Tetrahedron Lett., 5803 (1968); C. G. Swain and E. R. Thornton, J . Org. Chem., 26,4808 (1961); L. L. Brown and J. S.Drury, J . Chem. Phys., 43,1688 (1965). (3) Y.Yukawa, T. Ando, K. Token, M. Kawada, and S. G. Kim, Tetrahedron Lett., 2367 (1969).

Journal of the American Chemical Society

Reproducible to about 57& Calculated from the activity values of the starting ketone and the product ester or recovered ketone, respectively, a t various fractions of reaction; average deviation of values from various fractions of reaction +O. 002-0.003 except for p-CN, f0.006.

phenyl-l-14C acetates (2) and to point out the implications of these results for the mechanism of the reaction. 0

1

X-@G!CH,

U

It

+

RCO,H

2

The labeled acetophenones were prepared from commercially available (ring labeled) benzoic-1- 14C acid and p-nitrobenzoic-1- 14C acid by standard metho d ~ ~or - as ~ described el~ewhere.~The kinetic and isotope effect measurements were carried out in chloroform at 32 -f 0.1". The fraction of reaction was determined by standard iodometric methods and checked, with substantially identical results, by gas chromatographic or nmr analyses of the ketone/ester ratios. N o trace of the methyl benzoate esters could be found, despite a careful search by gas chromatography. p-Nitroacetophenone could not be oxidized to the corresponding ester under these conditions. All of the compounds studied displayed good secondorder kinetics, in contrast to the observation of Friess and Solowaylo that the related perbenzoic acid oxidation of substituted acetophenones displayed various kinetic orders depending on the substituent. It is clear the reaction is accelerated by electron-donating groups and slowed by electron-withdrawing groups, in general agreement with the results of Hawthorne and Emmons" on the related trifluoroperacetic acid oxidation of parasubstituted acetophenones. In Hammett plots of the kinetic data, the linear fit is better with u+ ( p = - 1.36) than with u, suggesting an activated complex which is electron deficient at a position capable of interaction with the para substituent. There is no indication of curvature in the Hammett plot, which supports the thesis that all of the compounds are reacting by the same mechanism. (4) R. E. Bowman, J . Chem. Soc., 322 (1950). (5) A. I. Vogel, "A Textbook of Practical Organic Chemistry," Longmans, Green, New York, N. Y., 1948, pp 576, 585, 647. (6) M. Sulzbacher, E. Bergman, and E. R. Pariser, J . Amer. Chem. SOC.,70, 2827 (1948). (7) L. I. Smith in "Organic Synthesis," Coll. Vol. 11, A. H. Blatt, Ed., Wiley, New York, N. Y., 1943, p 360. (8) Full details are given in the Ph.D. dissertation of B. W. P. * (9) B. W. Palmer and A. Fry, J . Label. Compounds, in press. (10) S. L. Friess and A. H. Soloway, J . Amer. Chem. Soc., 73, 3968 (1951). (11) M. F. Hawthorne and W. D. Emmons, ibid., 80,6398 (1958).

1 92:8 1 April 22, 1970

2581

For each compound, isotope effect measurements were made at five fractions of reaction, ranging from 8 to 60%. The reaction mixtures were quenched with sodium hydroxide solution. For 14C assay using a Beckman LSlOO liquid scintillation counter,Ethe phenols resulting from basic hydrolysis of the recovered acetates were converted t o benzoates and the recovered unreacted ketones were converted to oximes. The internal consistency of the isotope effect data is high, as evidenced by the relatively small errors, by the lack of any trend in k12/k14with fraction of reaction, and by the excellent agreement in the k12/k14 values calculated separately from the decrease in radioactivity of product ester and the increase in radioactivity of the recovered ketone. Most features of the mechanism of the peracid oxidation of ketones to esters are reasonably well understood.12 For most, if not all, cases the reaction is first order in peracid and first order in and is general acid catalyzed. 11,14 The migrating group does so with retention of configuration, l 5 and electrondonating substituents in the migrating group speed the reaction.’o*l 2 The ketone oxygen becomes the carbonyl oxygen of the ester.’O Our version of the Criegee rnechanisml7 may be applied to the present case as shown in eq 1. 1-

RCO,H

H+

OH

dOCR I1

I

3

The main question of timing is whether electrondeficient species 4 actually exists or whether 3 is converted to 2 (or its conjugate acid) by a concerted process. Although no previous research is definitive, most previous studies, especially that of Hawthorne and Emmons,” support a concerted reaction mechanism. The present isotope effect results lead unambiguously to the conclusion that the present reaction is concerted. No isotope effect would be expected for rate-determining formation of 3 or 4 since those steps do not involve significant alteration of the bonding at the labeled position.1s Since a large isotope effect is found, neither formation of 3 nor its decomposition to 4 can be rate determining. On the other hand, in the rate-determining concerted conversion of 3 to 2, bonding at the labeled position is extensively altered, and an isotope effect would be expected,ls as is observed. (Of course the possibility exists that a different step might be rate determining for other compounds or conditions.) The activated complex (5) for this concerted reaction may (12) Previous literature is very well reviewed by M.

F. Hawthorne,

W. D. Emmons, and K. S . McCallum, J . Amer. Chem. Sac., 80, 6393 ( 1958).

(13) Y . Yukawa and T. Yokoyama, J . Chem. SOC. Jap., 73, 371 ( 19 52).

(14) W. E. Doering and L. Spears, J. Amer. Chem. Soc., 72, 5515 ( 1950). (15) K. Mislow and J . Brenner, ibid., 75,2319 (1953). (16) W. E. Doering and E. Dorfman, ibid., 75,5595 (1953). (17) R. Criegee, Justus Liebigs Ann. Chem., 560, 127 (1948). (18) For a qualitative review of the general concepts leading to this

conclusion, and for leading references to the basic theory, see A. Fry, Pure Appl. Chem., 8 , 409 (1964).

be formulated as being similar to that suggested by Hawthorne and Emmons.

6+

6H

5

The variation of isotope effect with substituent, which is far larger than the variations observed in any previous work, can be rationalized in terms of activated complex 5. Increased bonding at a labeled position in an activated complex relative to reactants results in a decreased isotope effect; decreased bonding has the opposite effect. l8 In considering the bonding of the labeled ring carbon with the carbon at the migration origin and the oxygen at the migration terminus as the ring moves from one to the other, it is clear that different substituents will be able to satisfy the electron deficiency in the three-membered ring more or less readily. A good electron-donating group like methoxy will result in a high electron density in the three-membered ring, resulting in a “tight” activated complex with increased bonding between the ring carbon and the migration origin and terminus. This is equivalent to saying that the activated complex force constants at the labeled position are increased, and this results in a lowered isotope effect. An electron-withdrawing group will have the opposite effect, leading to a “loose” activated complex and a high isotope effect. This is exactly the trend observed experimentally. Because of the relative positions of the substituent, the labeled atom, and the electron-deficient center, a system such as the present one offers maximum opportunity for substituents to influence the isotope effect. (19) (a) National Science Foundation Trainee, 1965-1969; whom correspondence should be addressed.

(b) to

Billy W. Palmer,lg8Arthur Frylgb Department of Chemistry, University of Arkansas FayetteuiUe, Arkansas 72701 Received January 12, 1970

Structure and Stereochemical Behavior of Asymmetric a8ulfonyl Carbanions Sir: Two monobromo diastereomers, mp 76” and 112”, have been obtained by bromination of either dl- or meso-bis-a-methylbenzyl sulfone with N-bromosuccinimide. Single-crystal X-ray analysis using counter data has shown that the higher melting isomer has the erythro configuration 1, crystallizing in space group P2& All of the atoms were successfully located on a three-dimensional Fourier map phased by the bromine atom, and R = 0.06 for 1500 reflections above background. Reduction of 1 with sodium sulfite or triphenylphosphine in methanol occurred in a highly stereoselective manner (90 or more) to give bis-a-methylbenzyl sulfone, mp 140”, which has been shown to be the meso isomer (3). Similarly, threo-a-bromo-a-methylbenzyl ( 1 ) C. Y.Meyers and A. M. Malte, J . Amer. Chem. Sac., 91, 2123 (1969).

Communications to the Editor